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杨培强,陈炜,艾泽,等. xxxx. 武汉市后官湖局地气候效应的数值模拟研究[J].暴雨灾害,xx(x):xx-xx. DOI: 10.12406/byzh.2023-272
引用本文: 杨培强,陈炜,艾泽,等. xxxx. 武汉市后官湖局地气候效应的数值模拟研究[J].暴雨灾害,xx(x):xx-xx. DOI: 10.12406/byzh.2023-272
YANG Peiqiang, CHEN Wei, AI Ze, et al. xxxx. Numerical simulation study on local climate effects of Houguan Lake in Wuhan [J]. Torrential Rain and Disasters,xx(x):xx-xx. DOI: 10.12406/byzh.2023-272
Citation: YANG Peiqiang, CHEN Wei, AI Ze, et al. xxxx. Numerical simulation study on local climate effects of Houguan Lake in Wuhan [J]. Torrential Rain and Disasters,xx(x):xx-xx. DOI: 10.12406/byzh.2023-272

武汉市后官湖局地气候效应的数值模拟研究

Numerical simulation study on local climate effects of Houguan Lake in Wuhan

  • 摘要: 城市内湖对城市生态和人居环境作用显著,为研究武汉市内湖泊的局地气候效应,基于武汉市后官湖周边国家站观测资料和NCEP/FNL再分析资料,利用WRF数值模式开展冬、夏季典型月(2013年1月、7月)后官湖水体对湖区及周边地区地面气温、风速、相对湿度和降水量的影响和可能机制分析。结果表明:(1) 冬季典型月后官湖增温作用显著,夏季典型月则呈现弱增温作用。白天后官湖表现为冷湖效应,夜间表现为暖湖效应,日高温的降低和日低温的升高导致昼夜温差减小。(2) 后官湖对湖区的平均风速和平均日极大风速均有增大作用,冬季典型月后官湖对湖区与下风向区域平均风速和平均日极大风速的增大量和增大区域明显大于夏季典型月。(3) 后官湖在冬、夏两季典型月均有一定的“湿岛效应”,相对湿度随湖泊边界距离的增加而下降。而后官湖对湖区及周边地区降水量的影响很小。(4) 湖泊与陆地的气温差异导致湖区风向发生昼夜转变。湖体的大小、环境风场的变化与湖泊的局地气候效应密切相关。后官湖东南部湖体更大,对温度、风速、相对湿度影响的强度和范围更大。冬季典型月后官湖受偏北气流作用,对湖体南岸的气温、相对湿度的影响更显著,夏季典型月该特征反之。

     

    Abstract: The roles of urban inner lakes in changing the urban ecology and human living environment are significant, to study the local climate effect of lakes in Wuhan, based on the routine observation data of national stations around Wuhan Houguan Lake and the NCEP/FNL reanalysis data, the WRF numerical model was used to carry out the possible mechanisms of the impact of Houguan Lake on the surface temperature, wind speed, relative humidity and precipitation in the lake area and the surrounding areas during the typical months (January and July 2013) in winter and summer separately. The results are as follows: (1) In the typical months of winter, the warming effect of Houguan Lake is significant, while in the typical months of summer, the warming effect is weak. The Houguan Lake shows a cold lake effect in the daytime and a warm lake effect at night, and the decrease of the daily highest temperature and the increase of the daily lowest temperature lead to the decrease of the diurnal temperature difference. (2) The average wind speed and average daily maximum wind speed in the lake area are increased by Houguan Lake. In the typical months of winter, the region and value of the average wind speed and daily maximum wind speed in Houguan Lake area and downwind area increase significantly greater than that in the typical months of summer. (3) There is a limited "wet island effect" in Houguan Lake in both typical months of winter and summer. The relative humidity decreases with the increase of the lake boundary distance. Houguan Lake has a small impact on precipitation in the lake area and surrounding areas. (4) The temperature difference between the lake and the land leads to the diurnal conversion of the wind direction in the lake area. The size of the lake and the changes of environmental wind field are closely related to the local climate effects of the lake. The southeastern part of the lake is relatively larger, which has a greater intensity and range of impact on temperature, wind speed and relative humidity. In the typical months of winter, Houguan lake is affected by northerly airflow, which has a more significant impact on the temperature and relative humidity on the south bank of the lake. In the typical months of summer, this feature is reversed.

     

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